Abstract

Given the challenges to life at low pH, an analysis of inorganic sulfur compound (ISC) oxidation was initiated in the chemolithoautotrophic extremophile Acidithiobacillus caldus. A. caldus is able to metabolize elemental sulfur and a broad range of ISCs. It has been implicated in the production of environmentally damaging acidic solutions as well as participating in industrial bioleaching operations where it forms part of microbial consortia used for the recovery of metal ions. Based upon the recently published A. caldus type strain genome sequence, a bioinformatic reconstruction of elemental sulfur and ISC metabolism predicted genes included: sulfide–quinone reductase (sqr), tetrathionate hydrolase (tth), two sox gene clusters potentially involved in thiosulfate oxidation (soxABXYZ), sulfur oxygenase reductase (sor), and various electron transport components. RNA transcript profiles by semi quantitative reverse transcription PCR suggested up-regulation of sox genes in the presence of tetrathionate. Extensive gel based proteomic comparisons of total soluble and membrane enriched protein fractions during growth on elemental sulfur and tetrathionate identified differential protein levels from the two Sox clusters as well as several chaperone and stress proteins up-regulated in the presence of elemental sulfur. Proteomics results also suggested the involvement of heterodisulfide reductase (HdrABC) in A. caldus ISC metabolism. A putative new function of Hdr in acidophiles is discussed. Additional proteomic analysis evaluated protein expression differences between cells grown attached to solid, elemental sulfur versus planktonic cells. This study has provided insights into sulfur metabolism of this acidophilic chemolithotroph and gene expression during attachment to solid elemental sulfur.

Highlights

  • Inorganic sulfur compounds (ISCs) in acidic, sulfide mineral environments are produced as a result of abiotic Fe(III) oxidation of sulfide minerals such as pyrite (FeS2; initial inorganic sulfur compound (ISC) product is thiosulfate) or chalcopyrite (CuFeS2; initial product is polysulfide sulfur)

  • Bioinformatic reconstruction of A. caldus ISC metabolism Genes and metabolic pathways involved in ISC and S0 oxidation/reduction were obtained from Metacyc1 and Kegg2

  • Bioinformatic reconstruction of A. caldus ISC metabolism A detailed analysis of the genes present in the draft genome sequence of A. caldusT revealed genes for ISC oxidation that are common to A. ferrooxidans [sulfide quinone reductase, doxD, and tth] (Valdes et al, 2008) and other microbial representatives from extreme acidic environments

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Summary

Introduction

Inorganic sulfur compounds (ISCs) in acidic, sulfide mineral environments are produced as a result of abiotic Fe(III) oxidation of sulfide minerals such as pyrite (FeS2; initial ISC product is thiosulfate) or chalcopyrite (CuFeS2; initial product is polysulfide sulfur). As a result of sulfuric acid production, sulfide mineral environments are typically inhabited by acidophilic microorganisms These microorganisms are exploited in the biotechnological process of “Biomining” whereby dissolution of sulfide minerals is catalyzed by the action of ISC oxidizing microorganisms as well as Fe(II) oxidizers that regenerate the Fe(III) required for the abiotic attack of sulfide minerals (Rawlings and Johnson, 2007). Microorganisms utilize several systems for ISC oxidation including the Paracoccus pantotrophus 15 gene sulfur oxidizing (sox) cluster. This cluster encodes the multiple substrate Sox system that catalyzes oxidation of thiosulfate, elemental sulfur (S0), sulfide, and sulfite to sulfate. Due to the lack of Sox(CD), S0 is polymerized to form globules which can be further oxidized by proteins encoded in the dissimilatory sulfite reductase (dsr) gene cluster (Hensen et al, 2006)

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